Geosphere to atmosphere is the transition described in the volcanic eruption.
The geosphere is made up of rocky materials of different nature and that present different dynamics among themselves that were formed during convulsive stages of volcanic activity.
- The volcanic eruption is an emission of magma (mass of molten rocks, liquids and gases) that is found in the depths of the Earth where the temperature is extremely hot.
- In explosive eruptions, magma retains a large amount of gases, acquires greater pressure as it rises to the earth's surface and exits with great force.
- The diameter of the ash impact affects the earth's surface and the atmosphere causing lasting changes in the climate.
- Depending on the composition of the magma that has dissolved carbon dioxide, it can affect temperatures by making them hotter or colder than usual.
Therefore, we can conclude that geosphere to atmosphere is the transition described in the volcanic eruption.
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